Antarctic glaciers show seasonal behaviour, flows faster in summer: Studytext_fields
London: The mix of melting snow and warmer ocean waters causes glaciers along Antarctica's coastline to flow more quickly in the summer, according to a recent study.
The glaciers, or enormous chunks of flowing ice, move an average of about one kilometre per year.
But the study has found a seasonal variation in the speed of the ice flow, which speeded up by up to 22 per cent in summer when temperatures are warmer.
This gives an insight into the way climate change could affect the behaviour of glaciers and the role they could play in raising sea levels, the study said.
The paper is published in the journal Nature Geosciences.
Up to now, the study of the rugged Antarctic peninsula has been limited because of the difficulties scientists face getting onto the glaciers to conduct fieldwork.
But from space, advances in satellite technology are revealing new insights into the speed at which the glaciers are moving and draining water into the surrounding ocean.
The Antarctic Peninsula is the largest reservoir of frozen water on Earth.
It is estimated that between 1992 and 2017, melt water from the glaciers increased global sea levels by around 7.6 mm.
How that may change in the future is one of the big uncertainties in modelling climate change.
According to the study, a team of researchers, led by scientists at the University of Leeds, has used more than 10,000 satellite images, taken above the Antarctic Peninsula between 2014 and 2021, to understand how the flow of glaciers into the waters around the Antarctic alters during colder and warmer periods.
“One of the important findings of this study is that it reveals how sensitive glaciers in Antarctica are to the environment.
“We have known for a long time that glaciers in Greenland have a seasonal behaviour, but it is only now that satellite data has shown similar behaviour in Antarctica,” said the first author of the study, Ben Wallis.
The Antarctic Peninsula is the most northern and warmest region of Antarctica. It has a 1,000 km long mountainous spine, similar to the length of the east coast of Great Britain, and is home to a rich marine ecosystem of seals, penguins and whales.
Along the west coast of the peninsula, the glaciers drain ice from the ice sheet directly into the Southern Ocean.
Analysis of the satellite data showed that the glacier speed-up occurs in summer as the snow melts and the temperature of the waters in the Southern Ocean rise.
It is thought that water from the melting snow acts as a lubricant between the ice sheet and the underlying rock. As a result, friction is reduced and the speed at which the glaciers slide increases, the study said.
In addition, the warmer waters of the Southern Ocean erode the front of the moving ice, which reduces the buttressing forces it exerts to resist the ice flow, the study said.
“The Antarctic Peninsula has seen some of the most rapid warming of any region on Earth.
“Continuing work like this will help glaciologists monitor how quickly change is occurring, enabling accurate assessments of how Earth’s ice will respond to climate change,” said Anna Hogg, Associate Professor in the Institute for Climate and Atmospheric Science at Leeds and an author of the paper.
The European Space Agency and European Commission Copernicus Sentinel-1 satellite, whose data was used in this study, provides weekly monitoring around the whole coastline of Antarctica.
The satellite is fitted with synthetic aperture radar which can “see” through clouds, enabling measurements of the glaciers to be taken both day and night.
With PTI inputs